Articles | Volume 17, issue 12
https://doi.org/10.5194/bg-17-3223-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-3223-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Dissolved CH4 coupled to photosynthetic picoeukaryotes in oxic waters and to cumulative chlorophyll a in anoxic waters of reservoirs
Elizabeth León-Palmero
Departamento de Ecología and Instituto del Agua, Universidad de
Granada, 18071, Granada, Spain
Alba Contreras-Ruiz
Departamento de Ecología and Instituto del Agua, Universidad de
Granada, 18071, Granada, Spain
Ana Sierra
Departamento de Química Física and Instituto Universitario
de Investigación Marina (INMAR), Facultad de Ciencias del Mar y
Ambientales, Universidad de Cádiz, Puerto Real, 11510, Cádiz, Spain
Rafael Morales-Baquero
Departamento de Ecología and Instituto del Agua, Universidad de
Granada, 18071, Granada, Spain
Departamento de Ecología and Instituto del Agua, Universidad de
Granada, 18071, Granada, Spain
Research Unit “Modeling Nature” (MNat), Universidad de Granada, 18071, Granada,
Spain
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Cited
22 citations as recorded by crossref.
- Spatial Distribution of Dissolved Methane Over Extreme Oceanographic Gradients in the Subtropical Eastern South Pacific (17° to 37°S) L. Farías et al. 10.1029/2020JC016925
- The Hydration-Dependent Dynamics of Greenhouse Gas Fluxes of Epiphytic Lichens in the Permafrost-Affected Region O. Masyagina et al. 10.3390/f15111962
- “Greenhouse gas dynamics in a coastal lagoon during the recovery of the macrophyte meadow (Mar Menor, SE Spain)” B. Vallejo et al. 10.1016/j.scitotenv.2021.146314
- Magnitude and Drivers of Oxic Methane Production in Small Temperate Lakes S. Thottathil et al. 10.1021/acs.est.2c01730
- Potential role of submerged macrophytes for oxic methane production in aquatic ecosystems S. Hilt et al. 10.1002/lno.12095
- Understanding the fluxes of greenhouse gases in reservoirs under the inspiration of Margalef E. León-Palmero 10.23818/limn.42.22
- Linkages between greenhouse gases (CO2, CH4, and N2O) and dissolved organic matter composition in a shallow estuary V. Amaral et al. 10.1016/j.scitotenv.2021.147863
- Aerobic methane synthesis and dynamics in a river water environment A. Alowaifeer et al. 10.1002/lno.12383
- Microbial methane emissions from the non-methanogenesis processes: A critical review L. Liu et al. 10.1016/j.scitotenv.2021.151362
- High concentrations of dissolved biogenic methane associated with cyanobacterial blooms in East African lake surface water S. Fazi et al. 10.1038/s42003-021-02365-x
- Idiosyncratic phenology of greenhouse gas emissions in a Mediterranean reservoir E. Rodríguez‐Velasco et al. 10.1002/lol2.10409
- Practical Guide to Measuring Wetland Carbon Pools and Fluxes S. Bansal et al. 10.1007/s13157-023-01722-2
- P inputs determine denitrifier abundance explaining dissolved nitrous oxide in reservoirs E. León‐Palmero et al. 10.1002/lno.12381
- Picoplanktonic methane production in eutrophic surface waters S. Tenorio & L. Farías 10.5194/bg-21-2029-2024
- Phosphonate consumers potentially contributing to methane production in Brazilian soda lakes C. Carvalho et al. 10.1007/s00792-023-01318-y
- Biogeochemistry of Mediterranean Wetlands: A Review about the Effects of Water-Level Fluctuations on Phosphorus Cycling and Greenhouse Gas Emissions I. de Vicente 10.3390/w13111510
- Seasonal variations in dissolved CH4 and its controlling factors in two subtropical eutrophic reservoirs in China Y. Lv et al. 10.1007/s12517-022-09513-5
- Greenhouse gas emissions from Daihai Lake, China: Should eutrophication and salinity promote carbon emission dynamics? X. Li et al. 10.1016/j.jes.2022.12.021
- Candidatus Methylumidiphilus Drives Peaks in Methanotrophic Relative Abundance in Stratified Lakes and Ponds Across Northern Landscapes G. Martin et al. 10.3389/fmicb.2021.669937
- Particulate organic carbon sedimentation triggers lagged methane emissions in a eutrophic reservoir A. Martínez‐García et al. 10.1002/lol2.10379
- Reply to ‘Oxic methanogenesis is only a minor source of lake-wide diffusive CH4 emissions from lakes’ M. Günthel et al. 10.1038/s41467-021-21216-1
- Oxic methane production from methylphosphonate in a large oligotrophic lake: limitation by substrate and organic carbon supply L. Peoples et al. 10.1128/aem.01097-23
22 citations as recorded by crossref.
- Spatial Distribution of Dissolved Methane Over Extreme Oceanographic Gradients in the Subtropical Eastern South Pacific (17° to 37°S) L. Farías et al. 10.1029/2020JC016925
- The Hydration-Dependent Dynamics of Greenhouse Gas Fluxes of Epiphytic Lichens in the Permafrost-Affected Region O. Masyagina et al. 10.3390/f15111962
- “Greenhouse gas dynamics in a coastal lagoon during the recovery of the macrophyte meadow (Mar Menor, SE Spain)” B. Vallejo et al. 10.1016/j.scitotenv.2021.146314
- Magnitude and Drivers of Oxic Methane Production in Small Temperate Lakes S. Thottathil et al. 10.1021/acs.est.2c01730
- Potential role of submerged macrophytes for oxic methane production in aquatic ecosystems S. Hilt et al. 10.1002/lno.12095
- Understanding the fluxes of greenhouse gases in reservoirs under the inspiration of Margalef E. León-Palmero 10.23818/limn.42.22
- Linkages between greenhouse gases (CO2, CH4, and N2O) and dissolved organic matter composition in a shallow estuary V. Amaral et al. 10.1016/j.scitotenv.2021.147863
- Aerobic methane synthesis and dynamics in a river water environment A. Alowaifeer et al. 10.1002/lno.12383
- Microbial methane emissions from the non-methanogenesis processes: A critical review L. Liu et al. 10.1016/j.scitotenv.2021.151362
- High concentrations of dissolved biogenic methane associated with cyanobacterial blooms in East African lake surface water S. Fazi et al. 10.1038/s42003-021-02365-x
- Idiosyncratic phenology of greenhouse gas emissions in a Mediterranean reservoir E. Rodríguez‐Velasco et al. 10.1002/lol2.10409
- Practical Guide to Measuring Wetland Carbon Pools and Fluxes S. Bansal et al. 10.1007/s13157-023-01722-2
- P inputs determine denitrifier abundance explaining dissolved nitrous oxide in reservoirs E. León‐Palmero et al. 10.1002/lno.12381
- Picoplanktonic methane production in eutrophic surface waters S. Tenorio & L. Farías 10.5194/bg-21-2029-2024
- Phosphonate consumers potentially contributing to methane production in Brazilian soda lakes C. Carvalho et al. 10.1007/s00792-023-01318-y
- Biogeochemistry of Mediterranean Wetlands: A Review about the Effects of Water-Level Fluctuations on Phosphorus Cycling and Greenhouse Gas Emissions I. de Vicente 10.3390/w13111510
- Seasonal variations in dissolved CH4 and its controlling factors in two subtropical eutrophic reservoirs in China Y. Lv et al. 10.1007/s12517-022-09513-5
- Greenhouse gas emissions from Daihai Lake, China: Should eutrophication and salinity promote carbon emission dynamics? X. Li et al. 10.1016/j.jes.2022.12.021
- Candidatus Methylumidiphilus Drives Peaks in Methanotrophic Relative Abundance in Stratified Lakes and Ponds Across Northern Landscapes G. Martin et al. 10.3389/fmicb.2021.669937
- Particulate organic carbon sedimentation triggers lagged methane emissions in a eutrophic reservoir A. Martínez‐García et al. 10.1002/lol2.10379
- Reply to ‘Oxic methanogenesis is only a minor source of lake-wide diffusive CH4 emissions from lakes’ M. Günthel et al. 10.1038/s41467-021-21216-1
- Oxic methane production from methylphosphonate in a large oligotrophic lake: limitation by substrate and organic carbon supply L. Peoples et al. 10.1128/aem.01097-23
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Short summary
CH4 emissions from reservoirs are responsible for the majority of the climatic forcing of these ecosystems. The origin of the recurrent CH4 supersaturation in oxic waters is still controversial. We found that the dissolved CH4 concentration varied by up to 4 orders of magnitude in the water column of 12 reservoirs and was consistently supersaturated. Our findings suggest that photosynthetic picoeukaryotes can play a significant role in determining CH4 concentration in oxic waters.
CH4 emissions from reservoirs are responsible for the majority of the climatic forcing of these...
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